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Alex McColgan

๐Ÿ‘ค Speaker
See mentions of this person in podcasts
16246 total appearances

Appearances Over Time

Podcast Appearances

Astrum Space
All the Evidence We Have For Life on Mars

The sulphide needed to produce greigite could have come from volcanic gases leaking into groundwater.

Astrum Space
All the Evidence We Have For Life on Mars

But that means the sulphide would have had to migrate from a hot volcanic system into a much cooler environment, and there's been no evidence for such volcanic or hydrothermal sources nearby.

Astrum Space
All the Evidence We Have For Life on Mars

Another possibility is that sulfate in the rocks was reduced to sulfide through reactions with organic matter.

Astrum Space
All the Evidence We Have For Life on Mars

But unless temperatures exceed 150 to 200 degrees Celsius, these reactions would be very slow and require a huge amount of energy, making them unlikely.

Astrum Space
All the Evidence We Have For Life on Mars

and studies of the rocks around this area have shown no evidence of high temperatures.

Astrum Space
All the Evidence We Have For Life on Mars

So there's no way the surrounding environment could have got hot enough to reduce sulphate and form greigite.

Astrum Space
All the Evidence We Have For Life on Mars

Another possible explanation is acidity.

Astrum Space
All the Evidence We Have For Life on Mars

Both iron ions and sulfate ions dissolve much more readily in water under acidic conditions than they do under neutral conditions, making them much more prone to reduction through purely chemical reactions.

Astrum Space
All the Evidence We Have For Life on Mars

If the water on Mars was more acidic than we anticipated, that could have caused the spots Percy saw.

Astrum Space
All the Evidence We Have For Life on Mars

Perhaps these spots were just the result of chemical processes on an alien planet, nothing more.

Astrum Space
All the Evidence We Have For Life on Mars

But then, Percy spotted this little green mineral.

Astrum Space
All the Evidence We Have For Life on Mars

Nestled near the sample site, a small rock of olivine knocked the acidic water hypothesis on its head.

Astrum Space
All the Evidence We Have For Life on Mars

Olivine is the fastest-weathering silicate mineral.

Astrum Space
All the Evidence We Have For Life on Mars

Unlike other silicone structures like silicon dioxide, for example, olivine doesn't have strong silicon-oxygen-silicon bonds.

Astrum Space
All the Evidence We Have For Life on Mars

Instead, it's made up of negatively charged silicate ions held together by the electrostatic attraction with positively charged magnesium and iron ions.

Astrum Space
All the Evidence We Have For Life on Mars

In acidic conditions, these are displaced by hydrogen ions, breaking olivine down into orthosilicic acid and magnesium ions in solution.

Astrum Space
All the Evidence We Have For Life on Mars

The more acidic the environment, the more hydrogen ions there are, and the more aggressive the dissolution of olivine would be.

Astrum Space
All the Evidence We Have For Life on Mars

So the very fact that it exists rules out the possibility of acidic conditions causing the strange spots.

Astrum Space
All the Evidence We Have For Life on Mars

Science is ultimately about falsification.

Astrum Space
All the Evidence We Have For Life on Mars

It's not about proving a hypothesis true.